Not exact matches
There are more, however, including the amount
of sunlight an
ice sheet is able to reflect; the
larger an
ice sheet, the more sunlight is reflected, but the smaller an
ice sheet, the more ocean there is surrounding the
ice sheet to absorb the sunlight which in turn heats up the surrounding waters increasing the melt which decreases the size
of the
ice sheet which in turn... and so goes the cycle.
Using a cookie dough scoop or an
ice cream scoop
of medium size, scoop the cookies onto the prepared tray, 6 per
sheet (I baked a greater number per
sheet for the party because I was trying to bake such a
large number).
For
large cookies, use 1/4 cup (60 ml)(60 grams)
of batter (I like to use an
ice cream scoop) and place six cookies on each baking
sheet.
1) Mix flour, butter and
icing sugar in a bowl using two knives to cut the butter until the mixture resembles fine breadcrumbs 2) Add in the egg yolks and vanilla extracts and mix well, then add
iced water until the dough starts to come together 3) Shape the dough into a ball on a cool, flat, floured surface 4) Flatten dough into a disc and then wrap in plastic wrap, and chill in the refrigerator for at least 30 minutes 5) Meanwhile, peel, core and slice the apples into as thin slices as possible 6) Mix sugar and ground cinnamon powder with sliced apples and let it rest for a while 7) Pre-heat oven to 180 deg cel 8) Once dough has chilled, roll pastry dough on a
sheet of parchment paper until it has expanded to the size
of the tart mold (I used a rough mold the size
of a
large pizza) 9) Leaving at least an inch
of dough free, arrange apple slices by overlapping them slightly in the shape
of a circle, starting from the outermost part
of the circle, until you reach the inside 10) Fold the edges
of dough over the filling and then sprinkle the dough with a bit
of sugar 11) Bake for about 40 - 45 minutes, or until the crust is golden brown and the apples are soft 12) Serve warm, with a side
of whipped cream or
ice cream (optional)
Using a
large ice cream scoop, make balls
of ice cream and place them on the
sheet pan then return them to the freezer.
Pipe
icing in very thin, very straight lines across a parchment - lined baking
sheet, spacing close together (if
icing does not squeeze out
of bag easily, snip a slightly
larger opening).
Use an
ice cream scoop to dish out 8
large balls
of ice cream and then place them on a parchment paper lined
sheet pan
Drop approximately 1/4 cup portions
of the dough onto an un-greased cookie
sheet using an
ice cream scoop or
large spoon.
Once frozen pop the
ice out
of the container and put on a
large cookie
sheet.
Rest a balloon or beach ball on top
of a cone (use a small toy traffic cone, a
large funnel, or even just a
sheet of heavy paper rolled up) and have kids walk or run while keeping their
ice cream cone intact.
The governor, who has been around the state politics since the Laurentide
ice sheet retreated, knows something about the tortured relationship between the chief magistrate
of the state's
largest city and the state capital.
A
large area
of the Greenland
ice sheet once considered stable is actually shedding massive amounts
of ice, suggesting that future sea - level rise may be worse than expected, a team
of scientists warned yesterday in a new study.
Large areas
of the Earth's surface are experiencing rising maximum temperatures, which affect virtually every ecosystem on the planet, including
ice sheets and tropical forests that play major roles in regulating the biosphere, scientists have reported.
And over the past 18 months, two
of the peninsula's
largest ice shelves, the Larsen B and the Wilkins, have lost nearly 1,100 square miles
of their total area, a
sheet of ice about the size
of Rhode IslandCK.
This isn't the first time
ice sheets have calved from the Greenland mainland, but it's one
of the
largest breaks.
Even relatively
large calving events, where tabular
ice chunks the size
of Manhattan or bigger calve from the seaward front
of the shelf, can be considered normal if the
ice sheet is in overall balance.
ITS vast
ice sheets and monsoon run - off make the Tibetan plateau one
of the
largest sources
of fresh water on an increasingly thirsty planet.
«The fact that a
large portion
of the western flank
of the Greenland
ice sheet has become dark means that the melt is up to five times as much as if it was a brilliant snow surface.»
Co-author Professor Jonathan Bamber, based at the University
of Bristol, and President
of the European Geoscience Union (EGU), added: «We are seeing changes in the
large - scale circulation patterns, which leads to more frequent sunshine and higher amounts
of solar energy reaching the surface
of the
ice sheet.
The Dark Zone
of Greenland
ice sheet is a
large continuous region on the western flank
of the
ice sheet; it is some 400 kilometers wide stretching about 100 kilometres up from the margin
of the
ice.
Ice - sheet growth, coupled with favorable changes in Earth's orbit, pushed the planet past a climatic tipping point and led to both the rapid buildup of a permanent ice sheet in the Antarctic and much larger changes in global climate, says Hr
Ice -
sheet growth, coupled with favorable changes in Earth's orbit, pushed the planet past a climatic tipping point and led to both the rapid buildup
of a permanent
ice sheet in the Antarctic and much larger changes in global climate, says Hr
ice sheet in the Antarctic and much
larger changes in global climate, says Hren.
Buried under a
sheet of ice 2.5 miles thick, Lake Vostok is the world's seventh -
largest freshwater lake and the
largest of more than 300 lakes trapped beneath the Antarctic
ice sheet.
Some
of the variation the researchers found likely dates back to isolation
of different Hermit Thrushes populations by
ice sheets during the Pleistocene era, while differences between the two western groups may relate to body size, with
larger birds producing lower - frequency songs.
«The Ross
ice shelf for instance, is the main outlet for the West Antarctic Ice Sheet, which encompasses several large glaciers and contains the equivalent of five meters of sea level in its perched ice.&raq
ice shelf for instance, is the main outlet for the West Antarctic
Ice Sheet, which encompasses several large glaciers and contains the equivalent of five meters of sea level in its perched ice.&raq
Ice Sheet, which encompasses several
large glaciers and contains the equivalent
of five meters
of sea level in its perched
ice.&raq
ice.»
The slipperiness, caused by films
of water spread over
large areas, helps ascertain how quickly a melting
ice sheet will slide into the sea as the climate warms — and thus how quickly sea levels will rise.
Melting
of ice shelves does not directly contribute to sea - level rise, but instead they hold back water frozen in the
larger ice sheet that will cause sea levels to rise.
Greenland's
ice sheet melts and sends
large amounts
of fresh water into the coastal waters, where it is
of major importance for local production but potentially also for global ocean currents.
The
large Leverett Glacier, however, is more representative
of the glaciers that contribute the bulk
of meltwater coming from the Greenland
ice sheet, said Hawkings.
Traveling by helicopter from the main American base
of McMurdo Station on Ross Island to the Dry Valleys, researchers fly over a portion
of the Ross
Ice Shelf and then a corner
of the mesmerizing white spread
of the East Antarctic
Ice Sheet, which is the
largest in the world.
By 2100, the choice
of driving climate model conditions dominates the uncertainty, but by 2200, the uncertainty in the
ice sheet model and the elevation scheme are
larger.
It is not clear yet how much
of the phosphorus being released from the
ice sheet is reaching the open ocean, but if a
large amount
of phosphorus coming off the glacier makes it to the sea, the nutrient could rev up biological activity
of Arctic waters, according to the study's authors.
«By refining the spatial pattern
of mass loss in the world's second
largest — and most unstable —
ice sheet, and learning how that pattern has evolved, we are steadily increasing our understanding
of ice loss processes, which will lead to better - informed projections
of sea level rise.»
Totten Glacier, the
largest glacier in East Antarctica, is being melted from below by warm water that reaches the
ice when winds over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice of the East Antarctic Ice She
ice when winds over the ocean are strong — a cause for concern because the glacier holds more than 11 feet
of sea level rise and acts as a plug that helps lock in the
ice of the East Antarctic Ice She
ice of the East Antarctic
Ice She
Ice Sheet.
When
large parts
of the
ice sheet melted at the end
of the
ice age, the weight
of the
ice sheet decreased, and the crust began to rebound.
A March study shows that one
large swath
of the
ice sheet sits on beds as deep as 8,000 feet below sea level and is connected to warming ocean currents.
If the East Antarctic
ice sheet, which is 10 times
larger than the western
ice sheet, melted completely, it would cause sea levels worldwide to rise almost 200 feet, according to Kathy Licht, an associate professor in the Department
of Earth Sciences in the School
of Science at IUPUI.
On a clear day, anyone flying over Greenland on the route between North America and Europe can look down and see the bright blue patches
of melted water atop the flat, blindingly white expanse
of the
ice sheet that covers the island, the second
largest chunk
of ice on Earth.
The reason was that
ice sheets across Scandinavia and North America produced a
large amount
of fresh melt water from icebergs.
The continually dropping slope helps explain why northern Greenland, unlike Antarctica, has no
large subglacial lakes: Meltwater that either forms at the base
of Greenland's
ice sheet or ends up there after draining from the
ice sheet's upper surface flows away uninterrupted.
«It turns out that for much
of the East Antarctic
Ice Sheet's history, it was not the commonly perceived large stable ice sheet with only minor changes in size over millions of years,» he sa
Ice Sheet's history, it was not the commonly perceived large stable ice sheet with only minor changes in size over millions of years,» he
Sheet's history, it was not the commonly perceived
large stable
ice sheet with only minor changes in size over millions of years,» he sa
ice sheet with only minor changes in size over millions of years,» he
sheet with only minor changes in size over millions
of years,» he said.
Around 6 million years ago, the East Antarctic
Ice Sheet expanded, stabilized and ceased producing
large volumes
of meltwater.
It's one
of the
largest ice streams draining the West Antarctic
ice sheet, hundreds
of kilometres long and about 100 kilometres wide.
Based on the southern core we thought this was a localized low heat - flux region — but our model shows that a much
larger part
of the southern
ice sheet has low heat flux.
«During the last
ice age around 20,000 years ago,
large parts
of Canada were covered by an
ice sheet.
The East Antarctic
ice sheet is the
largest ice mass on Earth, roughly the size
of Australia.
We determine that this difference is driven by the growth and retreat
of large continental
ice sheets that are present in the cold
ice - age climates; these
ice sheets reflect a lot
of sunlight and their growth consequently amplifies the impact
of CO2 changes.»
Researchers at the University
of Washington and the University
of Edinburgh used data from the European Space Agency's CryoSat - 2 to identify a sudden drainage
of large pools below Thwaites Glacier, one
of two fast - moving glaciers at the edge
of the
ice sheet.
Jakobshavn Isbræ, which is widely believed to be the glacier that produced the
large iceberg that sank the Titanic in 1912, drains the Greenland
ice sheet into a deep ocean fjord on the coast
of the island.
But the
large volumes
of data on Arctic sea and land
ice that IceBridge has collected during its nine years of operations there have also enabled scientific discoveries ranging from the first map showing what parts of the bottom of the massive Greenland Ice Sheet are thawed to improvements in snowfall accumulation models for all of Greenla
ice that IceBridge has collected during its nine years
of operations there have also enabled scientific discoveries ranging from the first map showing what parts
of the bottom
of the massive Greenland
Ice Sheet are thawed to improvements in snowfall accumulation models for all of Greenla
Ice Sheet are thawed to improvements in snowfall accumulation models for all
of Greenland.
The Greenland
ice sheet is thought to be one
of the
largest contributors to global sea level rise over the past 20 years, accounting for 0.5 millimeters
of the current total
of 3.2 millimeters
of sea level rise per year.